CHEMISTRY · Stage 9 · Chapter 13: Planet Earth and Continental Drift
Chemistry Stage 9 Comprehensive Review
5 min read 6 parts Lesson 5 of 5
Lesson summary
Stage 9 Comprehensive Review — Alhussan International Academy — Chemistry (Stages 7–9) notes: Revise atomic structure, bonding, reaction types, rates and Earth science from Stage 9.Sodium — an atom is 2,8,1 and loses one electron to form Na+ (2,8).Sodium ion size — the ion is sma…
- Chloride ion size
- Ion formation
- Ionic compounds
- Simple molecular substances
- Giant covalent structures
- Balanced equations
Section 1 of 6Atoms and ions
- Sodium
- an atom is 2,8,1 and loses one electron to form Na+ (2,8).
- Sodium ion size
- the ion is smaller than the atom because the outer shell has been lost, so the remaining electrons are pulled in more strongly by the nucleus.
- Chloride ion size
- it is larger than a chlorine atom because adding an electron increases repulsion.
- Ion formation
- metals form positive ions, and non-metals form negative ions or share electrons in covalent bonds.
Section 2 of 6Structure and properties
- Ionic compounds
- giant lattices with high melting points.
- Simple molecular substances
- low melting points.
- Giant covalent structures
- very high melting points.
Section 3 of 6Reactions and salts
- Balanced equations
- balanced symbol equations show conservation of atoms, for example 2Mg + O2 → 2MgO.
- Making salts
- salts are made from acids with metals, oxides or carbonates, followed by filtration and crystallisation.
- Reactivity
- it decides displacement and extraction methods.
Section 4 of 6Rates of reaction
- Factors
- rate increases with higher concentration, temperature and surface area, because collisions become more frequent and, for temperature, more energetic.
- Investigating concentration
- change only the concentration, measure gas volume or time, and control temperature, mass and surface area of the metal.
| Topic | Key phrase |
|---|---|
| Ionic | Strong electrostatic forces between ions |
| Rate | More frequent effective collisions |
| Drift | Fossil and rock matches across oceans |
Section 5 of 6Rusting investigation and graphs
- Method
- iron nails are placed in tubes exposed to air and water at different temperatures, and the time for rust to appear is measured.
- Conditions
- rusting needs both oxygen and water, and higher temperatures usually speed it up.
- Graph
- put temperature on the x-axis and time on the y-axis, label both with units, plot points accurately and draw a smooth curve.
- Result
- the time falls as temperature rises, so the rate of rusting increases.
Section 6 of 6Earth science
- Wegener's hypothesis
- continental drift is supported by matching fossils, rock strata and the fit of the continents.
- Seafloor spreading
- new crust forms at mid-ocean ridges and moves outward, shown by magnetic stripes.
- Plate movement
- plates move a few centimetres a year and build mountains where they collide.
- Calculation
- multiply speed by time: a plate moving at 2 cm per year travels 200 cm (2 m) in 100 years.
- Use the data in the question, show working and write units.
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